Heat transfer-movement of energy from a warmer object to a cooler object
Three types:
Radiation-energy transfer through empty space
Convection-heat transfer by movement of a heated fluid
Conduction-heat transfer by movement of a heated fluid
Density-how much mass in a volume of a substance Convection currents-flow which transfers heat within a fluid
Outline:
Summary
heat is always transferred from a warmer substance to a cooler substance.
Radiation
heat transfer by radiation takes place with no direct contact between the heat source and the object
Conduction
the heated particles of a substance transfer heat to other particles through direct contact
Convection
during convection,heated particles of fluid being to flow,transferring heat energy from one part of the fluid to another
Convection in Earth's Mantle
Earth's mantle responds to heat
Convection Currents in Asthenosphere
convection currents have been moving for more than four billion years
at the top of the asthenosphere,hot material spreads out and pushes the cooler material out of the way,then the cooler material sinks back into the asthenosphere
Table of Contents
1.2 Convection Currents and the Mantle
Vocabulary:
Heat transfer-movement of energy from a warmer object to a cooler object
Three types:
- Radiation-energy transfer through empty space
- Convection-heat transfer by movement of a heated fluid
- Conduction-heat transfer by movement of a heated fluid
Density-how much mass in a volume of a substanceConvection currents-flow which transfers heat within a fluid
Outline:
Summary
Radiation
Conduction
Convection
Convection in Earth's Mantle